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1968 Inangahua Earthquake
The 1968 Inangahua earthquake struck west of Murchison, New Zealand, near the small town of Inangahua Junction at 5:24 am NZDT on 24 May 1968. The earthquake had a moment magnitude of 7.1, a local magnitude of 6.7, a surface wave magnitude of 7.4 and a maximum Mercalli intensity of X (''Exreme''). It occurred at a depth of , being extremely shallow for an earthquake of its size. It resulted in the deaths of three people, with a further 14 people injured, making it the fifth deadliest earthquake in New Zealand's recorded history (tied with the 1848 Marlborough earthquake). Numerous aftershocks followed the quake, including 15 that were magnitude 5 or greater and occurred within a month. Tectonic setting New Zealand lies along the boundary between the Indo-Australian and Pacific Plates. In the South Island most of the relative displacement between these plates is taken up along a single dextral (right lateral) strike-slip fault with a major reverse component, the Alpine ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Time In New Zealand
Time in New Zealand is divided by law into two standard time zones. The main islands use New Zealand Standard Time (NZST), 12 hours in advance of Coordinated Universal Time (UTC) / military M (Mike), while the outlying Chatham Islands use Chatham Standard Time (CHAST), 12 hours 45 minutes in advance of UTC / military M^ (Mike-Three). During summer months – from the last Sunday in September until the first Sunday in April – daylight saving time is observed and clocks are advanced one hour. New Zealand Daylight Time (NZDT) is 13 hours ahead of UTC, and Chatham Daylight Time (CHADT) 13 hours 45 minutes ahead. New Zealand's associated states – the Cook Islands and Niue – and the dependent territory of Tokelau use several different time zones at their own discretion. History On 2 November 1868, New Zealand officially adopted a standard time to be observed nationally, and was the first country to do so, about fifteen years before any other. Chatham Island was 45 minutes ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Buller Gorge
The Buller Gorge is a gorge located in the northwest of the South Island of New Zealand. The Buller River flows through the deep canyon between Murchison and Westport. Land Information New Zealand lists two sections for the gorge, Upper Buller Gorge and Lower Buller Gorge. runs alongside, but considerably above, the river through the gorge. The Stillwater - Westport Line railway also runs through the gorge. New Zealand's longest swingbridge at in length spans the Buller River west of Murchison. That area also offers rides on a zip-line across the gorge Buller Gorge Swingbridge Adventure and Heritage Park website. Accessed 2013-09-18. as well as several short bush walks. The gorge and river ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Earthquakes In New Zealand
This is a list of large earthquakes that have occurred in New Zealand. Only earthquakes with a magnitude of 6.0 or greater are listed, except for a few that had a moderate impact. Aftershocks are not included, unless they were of great significance or contributed to a death toll, such as the M 6.3 2011 Christchurch earthquake and the M 7.3 aftershock to the 1931 Hawke's Bay earthquake. Earthquakes occur frequently in New Zealand as the country is situated in the collision zone between the Indo-Australian and Pacific tectonic plates, part of the Pacific Basin Ring of Fire, where many earthquakes and volcanoes occur. Most events occur along the main ranges running from Fiordland in the southwest to East Cape in the northeast. This axis follows the boundary between the Indo-Australian and Pacific plates. Large earthquakes are less common along the central Alpine Fault, where the plates are not subducting and the forces are accommodated in different ways. The largest city within ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
1968 In New Zealand
The following lists events that happened during 1968 in New Zealand. Population * Estimated population as of 31 December: 2,773,000 * Increase since 31 December 1967: 28,000 (1.02%) * Males per 100 females: 99.8 – This was the first year (other than during a major war) in which the number of females exceeded the number of males. Incumbents Regal and viceregal *Head of State – Elizabeth II * Governor-General – Sir Arthur Porritt Bt GCMG GCVO CBE. Government The 35th Parliament of New Zealand continued, with the National government in power. *Speaker of the House – Roy Jack.Lambert & Palenski: ''The New Zealand Almanac'', 1982. *Prime Minister – Keith Holyoake *Deputy Prime Minister – Jack Marshall. *Minister of Finance – Robert Muldoon. *Minister of Foreign Affairs – Keith Holyoake. *Attorney-General – Ralph Hanan. * Chief Justice — Sir Richard Wild Parliamentary opposition * Leader of the Opposition – Norman Kirk (Labour). * Leader of the Socia ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Earthquakes In 1968
This is a list of earthquakes in 1968. Only magnitude 6.0 or greater earthquakes appear on the list. Lower magnitude events are included if they have caused death, injury or damage. Events which occurred in remote areas will be excluded from the list as they wouldn't have generated significant media interest. All dates are listed according to UTC time. Maximum intensities are indicated on the Mercalli intensity scale and are sourced from United States Geological Survey (USGS) ShakeMap data. There was a large resurgence in activity in 1968. 22 magnitude 7.0+ earthquakes struck various parts of the planet. The largest of these was a magnitude 8.2 event in Japan in May. Large aftershocks struck the area following the mainshock. New Zealand and Indonesia had some upheaval during the year. The high activity contributed to over 12,000 deaths across the world. The vast majority of this total was caused by a destructive event in Iran in August with nearly 10,500 deaths. Events in the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
UH-1H
The Bell UH-1 Iroquois military helicopter, first introduced in 1959, is the first production member of the prolific Huey family of helicopters, and was itself developed in over twenty variants, which are listed below. XH-40 and YH-40 The first Bell helicopter to use a turbine engine was a modified Model 47 (designated XH-13F), which had its initial flight in October 1954. The U.S. Army began a competition for a new helicopter for general utility and medical/casualty evacuation in 1955. In June 1955, Bell Helicopter was awarded a contract to develop the next generation turbine-powered utility helicopter for the U.S. Army. The resulting Bell Model 204 was designated XH-40 by the U.S. military and first flew on 22 October 1956. Two more prototypes were built in 1957, and six YH-40 pre-production helicopters were delivered in 1958.Donald, David, ed. "Bell 204". "Bell 205". ''The Complete Encyclopedia of World Aircraft''. Barnes & Nobel Books, 1997. . The YH-40's cabin was len ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bell UH-1H
The Bell UH-1 Iroquois (nicknamed "Huey") is a utility military helicopter designed and produced by the American aerospace company Bell Helicopter. It is the first member of the prolific Huey family, as well as the first turbine-powered helicopter in service with the United States military. Development of the Iroquois started in the early 1950s, a major impetus being a requirement issued by the United States Army for a new medical evacuation and utility helicopter. The Bell 204, first flown on 20 October 1956, was warmly received, particularly for the performance of its single turboshaft engine over piston engine-powered counterparts. An initial production contract for 100 ''HU-1A''s was issued in March 1960. In response to criticisms over the rotorcraft's power, Bell quickly developed multiple models furnished with more powerful engines; in comparison to the prototype's Lycoming YT53-L-1 (LTC1B-1) engine, producing 700 shp (520 kW), by 1966, the Lycoming T53-L- ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
RNZAF
The Royal New Zealand Air Force (RNZAF) ( mi, Te Tauaarangi o Aotearoa, "The Warriors of the Sky of New Zealand"; previously ', "War Party of the Blue") is the aerial service branch of the New Zealand Defence Force. It was formed from New Zealand elements of the British Royal Air Force, becoming an independent force in 1923, although many RNZAF aircrew continued to serve in the Royal Air Force until the end of the 1940s. The RNZAF fought in World War II, Malaya, Korean War, Vietnam and the Gulf War as well as undertaking various United Nations peacekeeping missions. From a 1945 peak of over 1,000 combat aircraft the RNZAF has shrunk to a strength of around 48 aircraft in 2022, focusing on maritime patrol and transport duties in support of the Royal New Zealand Navy and the New Zealand Army. The RNZAF's air combat capability ended in 2001, under the Fifth Labour Government with the disbanding of the A-4 Skyhawk and Aermacchi MB-339 based squadrons. The Air Force is led by an ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gisborne, New Zealand
Gisborne ( mi, Tūranga-nui-a-Kiwa "Great standing place of Kiwa") is a city in northeastern New Zealand and the largest settlement in the Gisborne District (or Gisborne Region). It has a population of The district council has its headquarters in Whataupoko, in the central city. The settlement was originally known as Turanga and renamed Gisborne in 1870 in honour of New Zealand Colonial Secretary William Gisborne. Early history First arrivals The Gisborne region has been settled for over 700 years. For centuries the region has been inhabited by the tribes of Te Whanau-a-Kai, Ngaariki Kaiputahi, Te Aitanga-a-Mahaki Rongowhakaata, Ngāi Tāmanuhiri and Te Aitanga-a-Hauiti. Their people descend from the voyagers of the Te Ikaroa-a-Rauru, Horouta and Tākitimu waka. East Coast oral traditions offer differing versions of Gisborne's establishment by Māori. One legend recounts that in the 1300s, the great navigator Kiwa landed at the Turanganui River first on the wa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Buller River
The Buller River ( mi, Kawatiri) is a river in the South Island of New Zealand. One of the country's longest rivers, it flows for from Lake Rotoiti through the Buller Gorge and into the Tasman Sea near the town of Westport. Within the Buller Gorge and downstream from the Deepdale River joining, the Buller crosses from Tasman District into Buller District. The Paparoa Range separates the Buller River from the Grey River. A number of flora and fauna are found in the Buller catchment, many of these extending onto the slopes of the Paparoa Range. The river is named after Charles Buller, Member of Parliament in the United Kingdom of Great Britain and Ireland (UK) and director of the New Zealand Company, a UK-based company in the early 1800s with a royal charter supporting colonization efforts of New Zealand. The original Māori name for the Buller is ''Kawatiri''. The Buller River upstream from Murchison along with the Mangles River are popular for whitewater kayaking and recre ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Reefton
Reefton is a small town in the West Coast region of New Zealand, some 80 km northeast of Greymouth, in the Inangahua River valley. Ahaura is 44 km south-west of Reefton, Inangahua Junction is 34 km to the north, Maruia is 63 km to the east, and the Lewis Pass is 66 km to the south-east. In 1888, it was the first town in New Zealand and the Southern Hemisphere to be lit by electricity, generated by the Reefton Power Station. Reefton was a thriving gold mining town in the late 19th century, and gold mining lasted from the 1870s to the 1950s. Its economy is based on tourism, forestry, coal mining and farming. Reefton is home to the Inangahua County Library. Name The rich veins of gold found in a quartz reef near the town led to its name, originally spelled "Reef Town". Two nicknames in use soon after it was founded were "Rest Town" and "Quartzopolis". The main street, Broadway, was named after West Coast magistrate Charles Broad. The nearby Wealth o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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